Petrogenesis of gem sapphire in a pegmatite-aplite vein from the Alvand batholith, Western Iran
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00710-020-00716-w.pdf
Reference74 articles.
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2. Agard P, Omrani J, Jolviet L, Whitechurch H, Vrielynck B, Spakman W, Monie P, Meyer B, Wortel R (2011) Zagros orogeny: a subduction-dominated process. Geol Mag 148:692–725
3. Ahadnejad V, Valizadeh MV, Deevsalar R, Rezaei-Kahkhaei M (2011) Age and geotectonic position of the Malayer granitoids: implication for plutonism in the Sanandaj–Sirjan zone, W Iran. Neues Jahrb Geol P-A 261:61–75
4. Alirezaei S, Hassanzadeh J (2012) Geochemistry and zircon geochronology of the Permian A-type Hasanrobat granite, Sanandaj–Sirjan belt: a new record of the Gondwana break-up in Iran. Lithos 151:122–134
5. Azizi H, Mohammadi K, Asahara Y, Tsuboi M, Daneshvar N, Mehrabi B (2016) Strongly peraluminous leucogranite (Ebrahim-attar granite) as evidence for extensional tectonic regime in the cretaceous, Sanandaj Sirjan zone, Northwest Iran. Chemie der Erde – Geochem 76:529–541
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3. Reply to the comment by F. Sajjadi Alehashem and M. Moazzen;Mineralogy and Petrology;2022-07-22
4. Comment on “Petrogenesis of gem sapphire in a pegmatite-aplite vein from the Alvand batholith, Western Iran” (2020) by R. Sheikhi Gheshlaghi, M. Ghorbani, A. A. Sepahi, R. Deevsalar and R. Shinjo;Mineralogy and Petrology;2022-06-09
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